在欧洲和北大西洋下方的地和上层地幔中绘制构造变形的地图
1Department of Geosciences, Princeton University, Princeton, NJ, USA. hejunzhu@princeton.edu
概括
我们创建了欧洲和北大西洋的3D地震模型,揭示了构造历史和石质层强度. 这种地震异构性为古代地质事件和当前板块运动提供了洞察力.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 构造学 构造学 构造学 构造学
背景情况:
- 了解地球的石质层需要详细的模型其物理性质.
- 地震异构性提供了关于地幔流动和岩石结构的关键信息.
研究的目的:
- 构建一个三维的欧洲和北大西洋的近向无极型模型.
- 为了将地震异构与历史上的构造事件和岩层强度相关联.
主要方法:
- 辅助地震断层扫描被用于构建异构模型.
- 进行了对异性质织物和强度配置文件的分析.
主要成果:
- 该模型显示了与北大西洋山脊延伸,地中海海沟撤退和安纳托利亚板块旋转相关的特征.
- 欧洲东北部下面的异构形状表明,这里有古老的裂系统.
- 确定了地下层的石质层强度和柔性流动.
结论:
- 地震异性反射反映了古老的构造事件和当前的地力学过程.
- 该模型有助于理解研究区域的石质层强度和变形机制.
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